Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/2516
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dc.contributorDepartment of Applied Physics-
dc.creatorXiang, R-
dc.creatorLung, MT-
dc.creatorLam, CH-
dc.date.accessioned2014-12-11T08:22:41Z-
dc.date.available2014-12-11T08:22:41Z-
dc.identifier.issn1539-3755-
dc.identifier.urihttp://hdl.handle.net/10397/2516-
dc.language.isoenen_US
dc.publisherAmerican Physical Societyen_US
dc.rights© 2010 The American Physical Society. The Journal's web site is located at http://pre.aps.org/en_US
dc.subjectAxisymmetricen_US
dc.subjectCritical radiusen_US
dc.subjectElastic strain energyen_US
dc.subjectFacetted surfacesen_US
dc.subjectFast kineticsen_US
dc.subjectHeteroepitaxyen_US
dc.subjectIsland formationen_US
dc.subjectLateral expansionen_US
dc.subjectLayer-by-layersen_US
dc.subjectNucleation energyen_US
dc.subjectNucleation mechanismen_US
dc.subjectQuantum Doten_US
dc.subjectSpontaneous formationen_US
dc.subjectThree-dimensional (3D) islandsen_US
dc.subjectTotal free energyen_US
dc.titleLayer-by-layer nucleation mechanism for quantum dot formation in strained heteroepitaxyen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage1-
dc.identifier.epage8-
dc.identifier.volume82-
dc.identifier.issue2-
dc.identifier.doi10.1103/PhysRevE.82.021601-
dcterms.abstractWe study the spontaneous formation of quantum dots in the form of three-dimensional (3D) islands on facetted surfaces in heteroepitaxy. Island development from fast kinetic Monte Carlo (KMC) simulations at low deposition rates is found to follow a layer-by-layer nucleation pathway characterized by energetics driven continuous lateral expansion interrupted by a sequence of independent two-dimensional (2D) upper-layer nucleation events. The process involves only unstable 2D upper-layer nuclei but no unstable 3D nucleus. We have calculated analytically the elastic strain energy of an island in the form of an axisymmetric stepped mound using a small-slope approximation. The total free energy of a system with a 3D island and an adatom bath is obtained. Our theory explains island formation via a free energy driven layer-by-layer nucleation mechanism. Upper-layer nucleation energy barrier, nucleation time, critical radius, and island step spacings are estimated. The relevance of entropic step-step repulsion is discussed. Our theory satisfactorily explains the 3D KMC simulations and may describe the initial evolution of islands in the form of stepped mounds observed in experiments.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationPhysical review. E, Statistical, nonlinear, and soft matter physics, 2 Aug. 2010, v. 82, no. 2, 021601, p.1-8-
dcterms.isPartOfPhysical review. E, Statistical, nonlinear, and soft matter physics-
dcterms.issued2010-08-02-
dc.identifier.isiWOS:000280487000003-
dc.identifier.scopus2-s2.0-77955578767-
dc.identifier.eissn1550-2376-
dc.identifier.rosgroupidr52965-
dc.description.ros2010-2011 > Academic research: refereed > Publication in refereed journal-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_IR/PIRAen_US
dc.description.pubStatusPublisheden_US
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